Calderas are important features in all volcanic environments and are commonly the sites of
geothermal activity and mineralisation. Yet, it is only in the last 25 years that a thorough …

The central-western Mediterranean area is a key region for understanding the complex
interaction between igneous activity and tectonics. In this review, the specific geochemical …

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In the past two decades, the central portion of Campi Flegrei caldera has experienced
ground uplift up to 15 mm/month, with an increase of rate, magnitude and extent of the …

Summary The∼ 150 km 3 (DRE) trachytic Campanian Ignimbrite, which is situated north-
west of Naples, Italy, is one of the largest eruptions in the Mediterranean region in the last …

This paper describes an approach to analyze ground deformation data collected by InSAR
(Interferometric Synthetic Aperture Radar) imaging the volcano feeding system (VFS) …

We have collected new stratigraphic data in the Campi Flegrei caldera through surface
geological map** and study of cores drilled to various depths. We integrate these data …

The Neapolitan Yellow Tuff (NYT) is the product of the largest known trachytic phreatoplinian
eruption. It covered an area larger than 1000 km2 with an estimated volume of about 40 km3 …

The Campi Flegrei caldera is a restless, nested structure resulting from two major collapses
related to the Campanian Ignimbrite (37,000 years BP) and the Neapolitan Yellow Tuff …

Geodetic observations at Campi Flegrei caldera were initiated in 1905. Historical
observations and the few measurements made before 1970 suggested a deflationary trend …